Estimación de la escorrentía superficial para el cálculo de la recarga a los acuíferos del macizo kárstico de los Ports de Beseit (Tarragona, España) combinando balance de agua en el suelo y análisis de hidrogramas de caudales

Hydrogeochemical, isotopic and geophysical characterization of saline lake systems in semiarid regions: The Salada de Chiprana Lake, Northeastern Spain

“…Water in the shallow piezometers shows a mean Cl content between of 666 and 704 mg/L (Table 3), whereas regional discharge from the Iberian Range mountain block has probably a Cl content b80 mg/L and corresponds to high elevation springs and mountain brooks, as it happens in the part of the Iberian Range to the east (Espinosa Martínez and Custodio, 2016). A coarse Cl balance points to a recharge in the Iberian Range that is higher than 15 mm/yr.…”